J Plant Ecol ›› 2026, Vol. 19 ›› Issue (5): rtag002.DOI: 10.1093/jpe/rtag002

   

Precipitation legacies reduce vegetation productivity and species diversity in semi-arid sandy grassland

Hongjiao Hu1,2, Xinping Liu1,*, Yuhui He1,3, Jiaqi Jing1,2, Yao Zhang1,2   

  1. 1 Inner Mongolia Naiman Agroecosystem National Field Observation and Research Station/State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
    2 University of Chinese Academy of Sciences, Beijing 100049, China;
    3 Lanzhou Ecological Agriculture Experimental Research Station/State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
    *Corresponding author. E-mail: liuxinping@lzb.ac.cn
  • Received:2025-10-13 Revised:2025-11-18 Accepted:2025-12-25 Published:2026-10-01
  • Supported by:
    This work was supported by the Inner Mongolia Autonomous Region Desert Control and Desertification Science and Technology Innovation Major Demonstration Project ‘Unveiling Commanding’ Project (2024JBGS0005-1); the Young Scholars Program on Regional Development, Chinese Academy of Sciences; and the Interdisciplinary Innovation Team Project of the Key Laboratory for Arid Land Ecological Security & Sustainability (E451890201).

降水遗留效应降低半干旱沙地草地植被生产力与物种多样性

Abstract: Precipitation legacy effects (PLEs) profoundly alter the recovery trajectories of semi-arid grasslands under global climate change, necessitating mechanistic quantification for accurate climate risk assessment in these vulnerable ecosystems. Based on a 7-year precipitation simulation experiment followed by an in situ natural recovery study in a semi-arid sandy grassland in Inner Mongolia, China, we characterized PLEs across multiple ecological hierarchies and varying precipitation patterns using data from the final treatment year and the first post-treatment year. Our results demonstrated that vegetation traits exhibited stronger PLEs than soil physicochemical properties. The magnitude of PLEs increased with higher functionalization (composition → productivity) and finer hierarchy (community → functional group), exceeding 50% when significant. Dry PLEs were generally stronger than wet PLEs; both exhibited bidirectional (positive/negative) performance, yet consistently showed an inverse relationship between vegetation traits and trait resilience. Mechanistically, PLEs of moderate wetting and extreme drying were primarily carried by vegetation-mediated information, whereas PLEs of moderate drying and spring drought legacies were mainly carried by soil-mediated material. Specifically, functional group composition served as the key information carrier: annuals primarily carried positive dry PLEs and negative wet PLEs, while perennials carried the opposite PLEs; and the prevalent negative PLEs in community-level productivity and species diversity were specifically attributed to perennial grasses expansion after drying and annual forbs expansion after wetting. Soil available nutrients acted as the key material carrier, promoting PLEs in annuals via synergistic physicochemical pathways. Overall, both dry and wet PLEs generally impeded the vegetation recovery of the sandy grassland ecosystem, despite positive effects on certain finer-hierarchy ecosystem traits. We conclude that ignoring PLEs may lead to a severe underestimation of climate change risks in semi-arid ecosystems, particularly regarding their most sensitive components.

Key words: precipitation pattern, legacy effect, ecological carrier, transgenerational memory, dominant functional group

摘要:
在全球变化背景下,降水遗留效应对半干旱草地恢复产生了深远影响,解析其内在机制对于评估该脆弱生态系统的气候风险至关重要。基于内蒙古半干旱沙地草地一项为期7年的降水控制实验及后续自然恢复研究,本研究利用降水处理最后一年和恢复后第一年的数据,揭示了不同降水处理下跨生态层级的遗留效应。研究发现,降水遗留效应对植被性状的影响强于土壤理化性质,并且从物种组成到生产力以及群落到功能群,该效应呈增强趋势,最高可超50%。此外,干旱遗留效应普遍强于湿润遗留效应;两者均表现出双向(正/负)作用,并且该效应在植被性状与性状恢复力间呈现负相关。在机制上,适度增水和极端干旱的遗留效应主由植被信息遗留载体承载,中度干旱和春季干旱则主由土壤遗留载体承载。具体而言,植物功能群组成是关键的信息载体:一年生植物主要承载正向干遗留效应及负向湿遗留效应,多年生植物则承载相反的遗留效应;并且,群落生产力和物种多样性整体上表现负向干湿遗留效应,主要归因于干旱后多年生禾草和湿润后一年生杂类草的扩张。土壤养分动态是关键的物质载体:其通过与其他土壤层面遗留载体的协同作用,显著促进了一年生植物遗留效应。总体而言,尽管干湿遗留效应对部分较细层级的生态系统属性存在正向作用,但二者总体上均阻碍了沙地草地植被的恢复。因此,若忽视降水遗留效应,将严重低估半干旱生态系统(尤其是敏感功能组分)所面临的气候风险。

关键词: 降水格局, 遗留效应, 生态载体, 隔代记忆, 优势功能群